Welcome to Visited Vertebrata Palasiatica, Today is

Most Download articles

    Published in last 1 year | In last 2 years| In last 3 years| All| Most Downloaded in Recent Month | Most Downloaded in Recent Year|

    In last 2 years
    Please wait a minute...
    For Selected: Toggle Thumbnails
    Teffichthys wui sp. nov., a new perleidid fish from the Early Triassic of Jiangsu and Anhui, China
    XU Guang-Hui, YUAN Zhi-Wei, REN Yi, LIAO Jun-Ling, ZHAO Li-Jun, SONG Hai-Jun
    Vertebrata Palasiatica    2024, 62 (3): 165-185.   DOI: 10.19615/j.cnki.2096-9899.240528
    Abstract669)   HTML89)    PDF(pc) (4514KB)(1419)       Save

    Perleididae is a group of stem neopterygian fishes known only from the Triassic. Here, we report the discovery of a new perleidid, Teffichthys wui sp. nov., based on six well-preserved specimens from the late Smithian (Olenekian, Early Triassic) marine deposits of Jurong, Jiangsu and Chaohu, Anhui, China. This new discovery documents the third and youngest species of Teffichthys , which is slightly younger than the Dienerian (Induan) T. elegans from Guizhou and the early Smithian T. madagascariensis from Madagascar. The new species shows diagnostic features of Teffichthys (presence of a spiracular, 38-41 lateral line scales, and no more than three epaxial rays in the caudal fin) but differs from T. madagascariensis and T. elegans in some autapomorphies (e.g., a horizontal opercle/subopercle contact and smooth scales with a nearly straight posterior margin). The diagnostic features for the genus Teffichthys and the family Perleididae are emended based on detailed comparisons of the new taxon with other perleidids. The phylogenetic relationships of perleidids with other stem neopterygians are discussed using a cladistic approach, and the results provide new insights into the phylogeny and classification of main stem neopterygian clades.

    Table and Figures | Reference | Supplementary Material | Related Articles | Metrics | Comments0
    Cranial anatomy of Anchiornis huxleyi (Theropoda: Paraves) sheds new light on bird skull evolution
    WANG Min, WANG Xiao-Li, ZHENG Xiao-Ting, ZHOU Zhong-He
    Vertebrata Palasiatica    2025, 63 (1): 20-42.   DOI: 10.19615/j.cnki.2096-9899.241225
    Abstract1117)   HTML43)    PDF(pc) (4662KB)(991)       Save

    The origin of birds from theropod dinosaurs, by any measures, is the most eye-catching evolutionary transition in the history of life, which encompasses numerous extensive morphological and biological changes. Compared to postcranium, little progress has been made regarding the evolutionary assemblage of the birds’ skull, because of few detailed early records of cranial materials of stem lineages. Anchiornis is the oldest known record of the Paraves (~160 Ma), the most inclusive clade that contains all living birds but not Caudipteryx or Epidexipteryx. With hundreds of known specimens, Anchiornis constitutes an ideal taxon for investigating morphological modifications across the theropod-bird transition, but its cranial morphology remains enigmatic. Here we present in-depth description of the cranial morphology of Anchiornis based on three-dimensional reconstruction of a well-preserved specimen, including elements from the temporal and palatal regions that are poorly recognized previously. Our study shows that Anchiornis retains the plesiomorphic dinosaurian condition in having a diapsid akinetic skull. The mixture of cranial characters, shared with dromaeosaurids, troodontids, and stemward avialans, present in Anchiornis demonstrates the complex history of early avialan cranial evolution.

    Table and Figures | Reference | Related Articles | Metrics | Comments0
    A small-sized dinocephalosaurid archosauromorph from the Middle Triassic of Yunnan, southwestern China
    WANG Wei, LEI Hong, LI Chun
    Vertebrata Palasiatica    2024, 62 (1): 13-32.   DOI: 10.19615/j.cnki.2096-9899.231013
    Abstract1128)   HTML60)    PDF(pc) (7822KB)(953)       Save

    Among numerous marine reptiles discovered in the Triassic eastern Tethys, today’s Southern China, Dinocephalosaurus is a bizarre animal comparable to European Tanystropheus in developing a prominently long neck. These two taxa are respectively assigned to Dinocephalosauridae and Tanystropheidae, and the two families and other basal members collectively form an early-diverging clade of Archosauromorpha. Here we report a new archosauromorph specimen, IVPP V18579, excavated from the lower Middle Triassic (Anisian), from Luoping, Yunnan in southwestern China. Compared with all the hitherto known dinocephalosaurids and tanystropheids, this skeletally mature individual is exclusively similar to Dinocephalosaurus in a number of characteristics, particularly with the long posterodorsal process of the premaxilla extending posteriorly beyond the level of the external nares, the concave posterior margin of the anteroposteriorly broad quadrate, and the strongly expanded distal end of the chevron in most of the caudal vertebrae. However, this reptile is much smaller than Dinocephalosaurus and different from Dinocephalosaurus and the other dinocephalosaurid, Pectodens, in many aspects, such as an anteriorly tapering long rostrum, the dentition composed of short conical teeth with less heterodonty, relatively but obviously tall neural spines of the axis and the anterior cervical vertebrae. Our phylogenetic analysis suggests that the new archosauromorph is a dinocephalosaurid, and then we erect Austronaga minuta gen. et sp. nov. based on this specimen. Detailed comparisons in osteological anatomy and the discussion about its potential aquatic adaptation of this new taxon are also provided.

    Table and Figures | Reference | Related Articles | Metrics | Comments0
    A new genus of galeaspids (jawless stem-Gnathostomata) from the early Silurian Chongqing Lagerstätte, China
    CHEN Yang, LI Qiang, ZHOU Zheng-Da, SHAN Xian-Ren, ZHU You-An, WANG Qian, WEI Guang-Biao, ZHU Min
    Vertebrata Palasiatica    2024, 62 (4): 245-261.   DOI: 10.19615/j.cnki.2096-9899.240820
    Abstract837)   HTML54)    PDF(pc) (6888KB)(941)       Save

    The early Silurian Chongqing Lagerstätte (middle Telychian) yields exceptionally preserved articulated jawless and jawed fishes. Here, we describe a new eugaleaspiform (Galeaspida, jawless stem-Gnathostomata), Miaojiaaspis dichotomus gen. et sp. nov., from the Chongqing Lagerstätte in Xiushan, Chongqing, China. The new form resembles Tujiaaspis vividus in the short medial dorsal canal, and the presence of the branching ends of the lateral transverse canal. They differ in that T. vividus has highly developed subordinate branches of the sensory canals that form a reticulate sensory canal system, and the median dorsal opening is more elongated. Our phylogenetic analysis recovers M. dichotomus and T. vividus as a monophyletic clade (Tujiaaspidae fam. nov.), which is supported by two synapomorphies: the short medial dorsal canal, and the branching ends of the lateral transverse canal. Tujiaaspidae forms a trichotomy with Shuyuidae and a clade comprising Anjiaspis, Sinogaleaspidae, Yongdongaspidae, and the ‘eugaleaspid cluster’. The sensory canal patterns in galeaspids are compared to show the transformation sequence of the sensory canal system in Eugaleaspiformes.

    Table and Figures | Reference | Supplementary Material | Related Articles | Metrics | Comments0
    The Late Miocene ‘ovibovin’ bovids in Eurasia
    Muhammad ILYAS, LI Qiang, SHI Qin-Qin, NI Xi-Jun
    Vertebrata Palasiatica    2024, 62 (4): 262-290.   DOI: 10.19615/j.cnki.2096-9899.240902
    Abstract745)   HTML51)    PDF(pc) (5776KB)(936)       Save

    During the Late Miocene, numerous medium to large-sized herbivores, that resemble the living Ovibos in skeletal morphology, dispersed throughout the Holarctic realm and comprised eleven genera: Lantiantragus, Shaanxispira, Tsaidamotherium, Criotherium, Mesembriacerus, Hezhengia, Urmiatherium, Parurmiatherium, Plesiaddax, Sinotragus, and Prosinotragus. These genera are primarily found in eastern Asia, in which nine genera are found in northern China, as well as in countries in eastern Europe and western Asia. They are distinguished by unique characteristics, including a perpendicular braincase, specialized horn cores, and a robust basioccipital. Previous studies have often classified these ‘ovibovin’ bovids as part of the conventional subfamily/tribe Ovibovinae/Ovibovini, along with extant Ovibos. Nevertheless, an increasing number of studies do not support the monophyly of the subfamily/tribe Ovibovinae/Ovibovini, nor is a close relationship likely between these Late Miocene ‘ovibovin’ bovids and extant Ovibos. Among the eleven genera of ‘ovibovin’ bovids, Plesiaddax, Hezhengia, and Urmiatherium are often considered to have a very close relationship and conventionally form the tribe Urmiatheriini. However, previous phylogenetic analyses do not support the monophyly of Urmiatheriini. This paper presents a summary of the transmutation of the terms Ovibovidae/Ovibovinae/Ovibovini/Ovibovina, the temporal and spatial distribution of the Late Miocene ‘ovibovin’ bovids in Eurasia, the principal characteristics of these taxa, and the previous phylogenetic analyses.

    Table and Figures | Reference | Related Articles | Metrics | Comments0
    A new small baurioid therocephalian from the Lower Triassic Jiucaiyuan Formation, Xinjiang, China
    LIU Jun, Fernando ABDALA
    Vertebrata Palasiatica    2024, 62 (3): 201-224.   DOI: 10.19615/j.cnki.2096-9899.240726
    Abstract606)   HTML31)    PDF(pc) (4011KB)(935)       Save

    Several therocephalian species, mainly represented by cranial material from the late Permian, have been reported from China in recent years. Here we describe a tiny new baurioid therocephalian, Jiucaiyuangnathus confusus gen. et sp. nov., from the Jiucaiyuan Formation, Xinjiang, China. The new taxon is represented by a partial snout with occluded partial lower jaw and two postcranial skeletons. Although juvenile in stage, the new species is diagnosed by the following features: round pit in middle of lateral surface of maxilla; lacrimal contact nasal; fossa for dentary tooth on the posterior end of the premaxilla, lateral to the anterior choana; two small vertical triangular ridges extending dorsally and ventrally on the vomerine anterior portion, and bordering a thin vomerine foramen laterally; anterior projection of the lateral part of the frontal on the nasal; symphyseal region of the dentary projected anteriorly; 5 upper premaxillary teeth, upper and lower canines absent, diastema between the last premaxillary upper incisor and first maxillary tooth present, no diastema separating anterior from posterior dentition in the mandible, 10 maxillary teeth and 12 dentary teeth, posterior postcanine expands mesiodistally, having a main large cusps and tiny anterior and posterior accessory cusps in line; neural arches of the atlas fused by the neural spine, neural spine of the axis projected posteriorly, procoracoid foramen lies between procoracoid and scapula. Features of the dentition resembles those of the small baurioid Ericiolacerta parva from South Africa and Silphedosuchus orenburgensis from Russia. The specimens provide the rare opportunity to know in detail the postcranial skeleton of baurioids.

    Table and Figures | Reference | Supplementary Material | Related Articles | Metrics | Comments0
    High-resolution CT-scan data reveals the tooth replacement pattern of the Late Jurassic tyrannosauroid Guanlong wucaii (Dinosauria, Theropoda)
    KE Yi-Hui, PEI Rui, XU Xing
    Vertebrata Palasiatica    2024, 62 (3): 225-244.   DOI: 10.19615/j.cnki.2096-9899.240715
    Abstract896)   HTML39)    PDF(pc) (2229KB)(894)       Save

    The Tyrannosauridae, which is characterized by specialized pachydont dentition and putative bone-cracking predatory strategies, is one of the most extensively studied theropod lineages. Although tooth replacement patterns, crucial for understanding feeding behaviors, have been thoroughly studied in this group, studies on non-tyrannosaurid tyrannosauroids are relatively scarce. This study utilizes high-resolution CT data to investigate the tooth replacement pattern in two specimens of Guanlong wucaii , a Late Jurassic tyrannosauroid, and provides insights into the evolution of tooth replacement across Tyrannosauroidea. Second-generation replacement teeth, a rarity observed mainly in giant predatory theropods (e.g. some tyrannosaurids), were detected in the dentary dentition of the juvenile Guanlong . Zahnreihen reconstructions display a consistent cephalad alternating tooth replacement pattern in the maxilla and the dentary of both of the examined individuals, with Z-spacing values exceeding 2.0. As Guanlong grows, the Z-spacing value in the maxillary dentition increases, resembling the ontogenetic changes documented in the Tyrannosauridae. Additionally, like Tarbosaurus , Guanlong also displays a discontinuity between the tooth replacement waves at the premaxilla-maxilla boundary. This study thus demonstrates that some tyrannosaurid-like tooth replacement patterns were acquired before the origin of the Tyrannosauridae.

    Table and Figures | Reference | Supplementary Material | Related Articles | Metrics | Comments0
    First report of Hispanodorcas from the Late Miocene of China
    WU Yong, WANG Shi-Qi, LIANG Zhi-Yong, GUO Ding-Ge, SUN Bo-Yang, LIU Long, DUAN Kai, CHEN Guo-Zhong
    Vertebrata Palasiatica    2024, 62 (2): 135-155.   DOI: 10.19615/j.cnki.2096-9899.240123
    Abstract461)   HTML40)    PDF(pc) (2487KB)(853)       Save

    As a small to middle-sized bovid, Hispanodorcas had previously only been found in the pan-Mediterranean region and South Asia. Its taxonomic classification at the tribe level has been a subject of debate, with possible associations to Antilopini, Reduncini, or Oiocerini. Here, we report on the first discovery of Hispanodorcas in East Asia, H. longdongica sp. nov. from the Daidian Locality in China, dating to the early Baodean age (~8-7 Ma). The new material consists of five skulls with varying states of preservation and provides the most complete osteological information on Hispanodorcas to date. It features a long, slender, and posteriorly curved horncore with a weak homonymous twist and both laterodorsal and medioventral grooves, which is characteristic of Hispanodorcas. This new species is characterized by having the smallest size amongst all known Hispanodorcas species, a weakly curved brain case in the facial region, and poorly developed posterior and anterior basilar tuberosities. These primitive characteristics suggest that H. longdongica may represent an early evolutionary stage of this genus. Furthermore, they indicate that Hispanodorcas might have directly evolved from the Gazella stock. The homonymous twist in the horncore, which aligns with Oiocerini, may be a case of homoplasy.

    Table and Figures | Reference | Related Articles | Metrics | Comments0
    Morphometric analysis of the cervical vertebral series in extant birds with implications for Mesozoic avialan feeding ecology
    LIU Bi-Ying, Thomas A. STIDHAM, WANG Xiao-Ping, LI Zhi-Heng, ZHOU Zhong-He
    Vertebrata Palasiatica    2024, 62 (2): 99-119.   DOI: 10.19615/j.cnki.2096-9899.240305
    Abstract890)   HTML35)    PDF(pc) (2040KB)(846)       Save

    The inference of Mesozoic avialan bird diets previously relied on traditional methods such as morphological comparisons among taxa and direct evidence such as identifiable stomach contents. However, the application of these approaches has been limited because of uncommon preservation of relevant fossil evidence. We searched for additional informative characteristics to help develop new methods to assess the diet of fossil birds. In particular, the morphology of the avialan neck is highly modularized and plays roles in multiple functions including food acquisition. The structure of and variation among the cervical vertebrae likely reflects the demands of feeding ecology in fossil and extant birds because the avialan neck evolved to, at least in part, replace the forelimbs by assisting with activities such as cranioinertial feeding and other ecological functions. Here, we utilize morphometric and statistical analyses to establish an initial quantitative relationship between cervical morphology and dietary modes in both extant and extinct birds. This morphometric framework derived from the cervical morphology of living birds is used as a basis to estimate the diet categories of five taxa of Mesozoic birds. The results indicate that there is a quantitative correlation between cervical morphology differentiation and their interrelated feeding modes. The enantiornithine taxa examined exhibit cervical morphologies similar to extant insectivorous or carnivorous birds. The ornithurine species show cervical morphologies that are more aligned with generalist or herbivorous birds, and exhibit preliminary morphological features tied to aquatic adaptions. These findings are consistent in part with other direct fossil evidence, as well as hypotheses developed from other skeletal comparisons. Therefore, the cervical vertebral series, as a skeletal system closely linked to food acquisition, can serve as one of the valuable metrics to provide information for inferring the diet of long extinct Mesozoic birds.

    Table and Figures | Reference | Supplementary Material | Related Articles | Metrics | Comments0
    Decline in phylogenetic diversity of Arthrodira (stem-group Gnathostomata) correlates with major Devonian bioevents
    XUE Qin-Yuan, YU Yi-Lun, PAN Zhao-Hui, ZHU You-An, ZHU Min
    Vertebrata Palasiatica    2024, 62 (1): 1-12.   DOI: 10.19615/j.cnki.2096-9899.231124
    Abstract600)   HTML64)    PDF(pc) (1062KB)(807)       Save

    Arthrodira, the most diverse subgroup of placoderms, or jawed stem gnathostomes, is noted for their occupation of high trophic levels, especially in the later stage of their evolutionary history. Despite the relatively complete fossil record of arthrodires, the results of previous studies on the arthrodire diversity, based on counting the numbers of taxa in each time interval (raw or taxic diversity), correlate poorly with major Devonian bioevents. Here, we assemble a new, exhaustive dataset of arthrodires, comprising 450 species of 219 genera. Most taxa are integrated into a supertree integrating the results from various phylogenetic investigations. Our analysis of the phylogenetic diversity, accounting for the presence of ghost lineages, reveals a very different pattern compared to the raw diversity. The phylogenetic diversity of arthrodires exhibited a typical early burst pattern, peaking in the Early Devonian (Lochkovian-Pragian Boundary), and followed by declines that aligned well with several major bioevents. Near each of the first four events, the arthrodire diversity experienced only minor drops and generally persisted at high levels. The later three events, particularly the Frasnian-Famennian Boundary and Devonian-Carboniferous Boundary Events, led to steep declines in arthrodire diversity, from which they never recovered before their complete extinction in the end-Devonian. All these declines were not evident in the raw or taxic diversity pattern, except that related to the Frasnian-Famennian Boundary Event.

    Table and Figures | Reference | Supplementary Material | Related Articles | Metrics | Comments0
    Osteology of Turfanodon bogdaensis (Dicynodontia)
    SHI Yu-Tai, LIU Jun
    Vertebrata Palasiatica    2024, 62 (3): 186-200.   DOI: 10.19615/j.cnki.2096-9899.240529
    Abstract487)   HTML35)    PDF(pc) (3320KB)(783)       Save

    Within the dicynodont genus Turfanodon , there are two recognized species, T. bogdaensis and T. jiufengensis . Both species are known by relatively complete cranial materials, but the mandibles and most postcranial bones have been described only for T. jiufengensis . This paper reports new dicynodont specimens from Turpan, Xinjiang, referring them to T. bogdaensis . They can clearly be differentiated from T. jiufengensis by the flatter lateral surface of the snout region, a prominent swelling on the lateral dentary shelf, and the rounded femoral head. The diagnosis of Turfanodon is revised. The combination of a flat circumorbital rim, posterior portion of anterior pterygoid rami with converging ventral ridges, and a possible autapomorphy, a deep notch on scapula forming procoracoid foramen, are confirmed. It also differentiated from all dicynodonts other than Myosaurus , Kembawacela and Lystrosaurus by having accessory ridges lateral to the median palatal ridge.

    Table and Figures | Reference | Related Articles | Metrics | Comments0
    A skull of Early Pleistocene Paracamelus gigas (Artiodactyla, Mammalia) from Luotuo Hill in Dalian, Northeast China
    DONG Wei, LIU Wen-Hui, BAI Wei-Peng, LIU Si-Zhao, WANG Yuan, LIU Jin-Yuan, JIN Chang-Zhu
    Vertebrata Palasiatica    2024, 62 (1): 47-68.   DOI: 10.19615/j.cnki.2096-9899.230616
    Abstract639)   HTML26)    PDF(pc) (2624KB)(773)       Save

    Originated in North America in the Middle Eocene, camelids were a successful group with very large diversity. But the camels emigrated to the Old World from North America, probably during the middle stage of the Middle Miocene, and did not radiate much as those in North America, represented by only two genera Paracamelus and Camelus. The former was considered as giving rise to the latter, but the detailed relationship of the Old World camelines was controversial. The new camel material unearthed from Layer 4 in the Jinyuan Cave at Luotuo Hill in Dalian, Liaodong peninsula in Northeast China, was described and referred to as Paracamelus gigas. Its dentition length is slightly longer than that of Camelus knoblochi but evidently larger than that of C. ferus and C. dromedarius. Based on the fossil records and morphometric evidences, P. gigas originated from a form similar to P. alexejevi in the Late Pliocene in the Old World, instead of from Megatylopus gigas of North America and then migrated into Asia as previously thought. The morphometric similarities between the Early Pleistocene Dalian specimens and those of the Middle and Late Pleistocene C. knoblochi indicate that P. gigas probably gave rise to C. knoblochi as formerly postulated and likely in the late Early Pleistocene by reduction or simplifying of P3 and P4, disappearance of p3 and shortening of dentition length. P. gigas inhabited in the forest steppe environment of Liaodong peninsula from 1.1 to 1.52 Ma based on paleomagnetic dating and pollen evidence.

    Table and Figures | Reference | Related Articles | Metrics | Comments0
    First Asian Paleocene pantolambdid pantodont (Mammalia) and its implications to intercontinental faunal exchange
    QUAN Shuo-Shuo, WANG Yuan-Qing
    Vertebrata Palasiatica    2024, 62 (4): 291-312.   DOI: 10.19615/j.cnki.2096-9899.240829
    Abstract699)   HTML60)    PDF(pc) (2248KB)(772)       Save

    Pantodonta was one of the first groups of eutherians to evolve at the beginning of Cenozoic era, including the largest herbivores at that time. Pantodonta shows considerable diversity during the Paleocene and Eocene, with most of the species having been discovered in Asia and North America. Here, we report on a new pantodont, represented by lower jaws with well-preserved dentition, discovered from the Middle Paleocene Nongshan Formation of the Nanxiong Basin, Guangdong Province, China. Its unique dental and mandibular characteristics distinguish it well from any known Asian pantodont, but are quite consistent with North American taxa, especially Pantolambda and Titanoides. The new specimen is identified as Nanxiongilambda yei gen. et sp. nov., characterized by the combination of the following morphological features: thick and robust mandible with a conspicuous anteroexternal flange, high positioned condyloid process, posteriorly protruding angular process, robust but not elongated lower canines, double-rooted p1, small but distinct talonids on posterior lower premolars, talonids nearly as wide as trigonids on lower molars, and m3 with a well-developed hypoconulid and a distinct entoconid. The new discovery marks the first record of a pantolambdid pantodont outside of North America, suggesting a broader geographical distribution and intercontinental dispersal of this clade during the Paleocene. Considering the more primitive Pantolambda only found from Torrejonian to early Tiffanian NALMA (equivalent to middle-late Shanghuan to early Nongshanian ALMA), which is slightly earlier than Nanxiongilambda (early Nongshanian ALMA), pantolambdids have likely undergone a particular wave of migration from North America to Asia during the Early-Middle Paleocene. Previous researches have suggested that pantodonts had dispersed only from Asia to North America during the Early Paleocene, but our new specimen indicates the biotic dispersal may have occurred in the opposite direction. The new specimen also contributes to the renewal of the evolutionary history of pantodonts and provides further insights into the migration and dispersal of Paleocene mammals.

    Table and Figures | Reference | Related Articles | Metrics | Comments0
    A taxonomical revision of ‘Dongfangaspis qujingensis’ from the Lower Devonian of Qujing, Yunnan Province
    SHAN Xian-Ren, ZHU Min, LI Qiang, GAI Zhi-Kun
    Vertebrata Palasiatica    2024, 62 (2): 85-98.   DOI: 10.19615/j.cnki.2096-9899.240321
    Abstract567)   HTML59)    PDF(pc) (3503KB)(719)       Save

    The affinity of ‘Dongfangaspis qujingensis’, initially assigned to Dongfangaspis but later to Laxaspis, has long been controversial. However, the taxonomical revision raises a new problem of junior homonym since the type species of Laxaspis is L. qujingensis. Here, we describe some new materials of ‘Dongfangaspis qujingensis’ and Damaspis vartus from the Xishancun Formation (early Lochkovian, Early Devonian) in Qujing, Yunnan Province. ‘Dongfangaspis qujingensis’ strikingly resembles Damaspis vartus in the slightly longer headshield, bifurcated ends of the lateral transverse canals, unconnected V-shaped posterior supraorbital canals, and at least seven pairs of lateral transverse canals issuing from the lateral dorsal canal. These similarities indicate that ‘D. qujingensis’ is more suggestive of Damaspis than Dongfangaspis and Laxaspis. Therefore, we propose to remove ‘Dongfangaspis qujingensis’ from Laxaspis to Damaspis. The new specimens of Damaspis vartus reveal five long lateral transverse canals on the right side, corroborating that the asymmetric sensory canal system in the holotype is the intraspecific variation.

    Table and Figures | Reference | Related Articles | Metrics | Comments0
    New material of Paukkaungmeryx minutus (Cetartiodactyla, Archaeomerycidae) from the late Middle Eocene Pondaung Formation, Myanmar
    Stéphane DUCROCQ, Yaowalak CHAIMANEE, Olivier CHAVASSEAU, Aung Naing SOE, Chit SEIN, Jean-Jacques JAEGER
    Vertebrata Palasiatica    2023, 61 (3): 182-197.   DOI: 10.19615/j.cnki.2096-9899.230522
    Abstract496)   HTML38)    PDF(pc) (3229KB)(708)       Save

    We describe here new dental material from the locality of Myaukse Kyitchaung (Pondaung Formation, central Myanmar) that we refer to the primitive Archaeomerycidae ruminant Paukkaungmeryx minutus Ducrocq et al. (2020). The upper molars are morphologically very similar to those of the holotype and exhibit only slight variations on features like the better development of buccal and lingual cingula. The lower teeth display primitive characters including a simple p4 and bunoselenodont lower molars that lack folds on the back of the trigonid wall. This additional material makes Paukkaungmeryx the second archaeomerycid in Pondaung known by upper and lower teeth material, and documents the apparently complex early evolution of the family.

    Table and Figures | Reference | Related Articles | Metrics | Comments0
    A possible new amphicyonid from the Miocene of the Linxia Basin
    JIANGZUO Qi-Gao, GAO Yuan, Alberto VALENCIANO, LU Dan, WANG Shi-Qi
    Vertebrata Palasiatica    2024, 62 (2): 156-164.   DOI: 10.19615/j.cnki.2096-9899.240320
    Abstract615)   HTML41)    PDF(pc) (3403KB)(694)       Save

    Here we report a new form of amphicyonid from an uncertain locality in the Linxia Basin. The derived dental traits imply an affinity to Magericyon, previously known from Europe and possibly southern Asia. The specimen suggests a higher diversity of amphicyonids in eastern Asia than previously thought, and more discovery with stratigraphic information will be needed to elucidate the evolution of Amphicyonidae in eastern Asia.

    Table and Figures | Reference | Related Articles | Metrics | Comments0
    The first discovery of non-avian dinosaur egg clutch (Macroolithus yaotunensis, Elongatoolithidae) from the Upper Cretaceous Qiupa Formation of Tantou Basin
    ZHU Xu-Feng, CHANG Fei, LI Yu, ZHANG Xu-Huang, GAO Dian-Song, WANG Qiang, QIU Rui, WANG Xiao-Lin, LIU Di, JIA Song-Hai, JIA Guang-Hui, ZHANG Jian-Hua, XU Li
    Vertebrata Palasiatica    2025, 63 (2): 159-172.   DOI: 10.19615/j.cnki.2096-9899.250212
    Abstract423)   HTML11)    PDF(pc) (9319KB)(642)       Save

    The Upper Cretaceous of Tantou Basin in western Henan has yielded many vertebrate fossils, which are featured by several non-avian dinosaurs. Meanwhile, studies on their eggs were yet inadequate though many eggshells have been reported. The newly discovered material 41HⅤ0199 was excavated from the Upper Cretaceous Qiupa Formation in 2021. The block preserves eight complete eggs arranged in two partial rings that form a partial clutch, and there are some scattered eggshells preserved closely with the block, showing a concave-up to concave-down ratio of 54.5 : 45.5, which indicates that the scattered eggshells come from the clutch and the clutch had been partially broken before it was buried. Based on morphological and microstructural characteristics, the eggs and eggshells can be assigned to Macroolithus yaotunensis (Elongatoolithidae), an oospecies known to be related to oviraptorids, which leads Yulong mini to be its probable producer. Besides, some eggshells show microstructural signs indicating egg retention, which marks the second example of egg retention in the oofamily Elongatoolithidae.

    Table and Figures | Reference | Related Articles | Metrics | Comments0
    Restudy of Rhinocerotini fossils from the Miocene Jiulongkou Fauna of China
    LI Shi-Jie, DENG Tao
    Vertebrata Palasiatica    2023, 61 (3): 198-211.   DOI: 10.19615/j.cnki.2096-9899.230630
    Abstract712)   HTML26)    PDF(pc) (1864KB)(629)       Save

    All the extant rhino species belong to Rhinocerotini and either have one horn (a nasal horn) or two horns (a nasal horn and frontal horn). So far, the earliest Rhinocerotini to have been identified in China is the “Dicerorhinuscixianensis, which was based on a juvenile skull with an associated mandible from the Middle Miocene locality of Jiulongkou in Cixian County, Hebei Province of northern China. Our analyses suggest that there are similarities between this specimen and the modern genus, Dicerorhinus, but it differs in several cranial traits and therefore cannot be assigned to the modern genus. Instead, it is closer to the Middle Miocene Lartetotherium from Europe, especially the specimen from La Retama in Spain and should be assigned to that genus, indicating the presence of intracontinental dispersal at this time. The Jiulongkou fauna is the only Middle Miocene fauna with Rhinocerotini in China, and, together with the faunal composition, this implies a more humid and closed environment, in contrast to those found in western China. We suggest that the position of the posterior border of the nasal notch is a good indication of the specimen’s evolutionary level in Rhinocerotini. The anterior position of the nasal notch as seen in modern Dicerorhinus, together with its certain similarities to L. cixianensis as well as its differences with more specialized species of the Dihoplus-Pliorhinus-Stephanorhinus -Coelodonta lineage, supports the conclusion that Dicerorhinus experienced little change during a nearly 10 Myr evolutionary history, possibly due to the low selection pressure seen in the tropical/subtropical forests in southeastern Asia.

    Table and Figures | Reference | Related Articles | Metrics | Comments0
    Sarcopterygians from the Lochkovian (Lower Devonian) of Nanning, Guangxi, China
    LI Mao-Kun, CUI Xin-Dong, ZHU Min, QIAO Tuo
    Vertebrata Palasiatica    2025, 63 (1): 1-19.   DOI: 10.19615/j.cnki.2096-9899.241226
    Abstract473)   HTML34)    PDF(pc) (5786KB)(587)       Save

    Here we report a left cheek plate of Psarolepis, a postparietal shield of Youngolepis, a skull of Diabolepis, and a scale of Styloichthys from the Lianhuashan and Nahkaoling formations (Lochkovian, Lower Devonian) of Nanning, Guangxi. This marks the first report of Diabolepis and Styloichthys beside Qujing, Yunnan, and the latest occurrence of Psarolepis to date. The fossil community displays significant similarities to the Xujiachong Assemblage, and provides new data for the Lower Devonian stratigraphic correlation between southwestern China and northern Vietnam. Given the latest dating constraint based on the conodont evidence, we regard that the Xujiachong Assemblage has a much longer range than previously supposed, extending from the latest Lochkovian to the end of Pragian. We propose that the transition of the Nahkaoling and Lianhuashan formations in Nanning might correspond to the Guijiatun Formation in Qujing. The relatively large size of fish individuals from Guangxi is probably attributed to the increase in the oxygen content of the ocean.

    Table and Figures | Reference | Related Articles | Metrics | Comments0
    Reassessment of Trilophodon connexus Hopwood, 1935 and attributing it to the Choerolophodontidae
    LI Chun-Xiao, CHEN Jin, WANG Shi-Qi
    Vertebrata Palasiatica    2024, 62 (1): 33-46.   DOI: 10.19615/j.cnki.2096-9899.230917
    Abstract410)   HTML20)    PDF(pc) (1602KB)(556)       Save

    Trilophodon connexus Hopwood, 1935 has long been considered a typical species of Gomphotherium in China. However, due to the unknown state of the mandibular symphysis and tusks, there is no definite evidence to assign “T. connexus” to Gomphotherium. Here we describe and reevaluate a hemimandible from the Halamagai Formation, Ulungur region, northern Junggar Basin, which was previously identified as Gomphotherium cf. G. shensiensis. The mandibular symphysis is deeply troughed and lacks mandibular tusks; therefore, it undoubtedly belongs to the Choerolophodontidae. Further comparison revealed that the cheek tooth morphology is identical to that of the type specimen of Trilophodon connexus. The characteristic features include high bunodonty, elongation of the m3 with four lophids, an only weakly chevroned lophid 2, enlargement of the posterior pretrite central conule 2, unfused state of the pretrite mesoconelet 2 (if present) and anterior pretrite central conule 2, as well as the absence of ptychodonty, choerodonty, and cementodonty. Therefore, T. connexus Hopwood, 1935 is a choerolophodontid rather than a species of Gomphotherium. Based on the above features, we provisionally refer to it as “Choerolophodonconnexus. “Choerolophodonconnexus is characterized by the following features: weak or absent ptychodonty, choerodonty, and loph chevron (which were all strong in the typical species of Choerolophodon), as well as multiplication of the lophids in the m3, which were similar to that of the North American Gnathabelodon. Therefore, Gnathabelodon might represent a distinct lineage within the Choerolophodontidae, and may be derived from the East Asian “Choerolophodonconnexus.

    Table and Figures | Reference | Related Articles | Metrics | Comments0
    Drishti Paint 3.2: a new open-source tool for both 2D and 3D segmentation
    WANG Meng-Jun, Ajay LIMAYE, LU Jing
    Vertebrata Palasiatica    2024, 62 (4): 313-320.   DOI: 10.19615/j.cnki.2096-9899.240619
    Abstract587)   HTML24)    PDF(pc) (1195KB)(548)       Save

    X-ray computed tomography (CT) has been an important technology in paleontology for several decades. It helps researchers to acquire detailed anatomical structures of fossils non-destructively. Despite its widespread application, developing an efficient and user-friendly method for segmenting CT data continues to be a formidable challenge in the field. Most CT data segmentation software operates on 2D interfaces, which limits flexibility for real-time adjustments in 3D segmentation. Here, we introduce Curves Mode in Drishti Paint 3.2, an open-source tool for CT data segmentation. Drishti Paint 3.2 allows users to manually or semi-automatically segment the CT data in both 2D and 3D environments, providing a novel solution for revisualizing CT data in paleontological studies.

    Table and Figures | Reference | Supplementary Material | Related Articles | Metrics | Comments0
    New suoid remains (Mammalia, Artiodactyla) from the Late Miocene of Haritalyangar, India
    Anek R. SANKHYAN, Olivier CHAVASSEAU
    Vertebrata Palasiatica    2024, 62 (1): 69-84.   DOI: 10.19615/j.cnki.2096-9899.231120
    Abstract337)   HTML24)    PDF(pc) (1762KB)(546)       Save

    We report here a number of mandibular, maxillary and dental fossil remains of Indian Suoidea from the Middle Siwalik of Haritalyangar area in Bilaspur District of Himachal Pradesh, North India. Haritalyangar is well known for the diversity of the Late Miocene fauna and the hominoids and other primates. The suoid remains were collected by one of the authors (ARS) during different field seasons and their localities were plotted on the map, along with those of the proboscidean reported recently, including the hominoid localities. The fossil localities are spread over the ‘Lower Alternations’ and the ‘Upper Alternations’ from Makkan Khad to Sir Khad. We have assigned the fossils into three genera, Propotamochoerus (P. hysudricus), Hippopotamodon (H. sivalense) and Yunnanochoerus (Y. dangari). Propotamochoerus hysudricus represents the most common suid in the Middle Siwaliks. The new remains of the suoid Yunnanochoerus dangari further documents this rare palaeochoerid only known in the Haritalyangar area by a few fossils. The new suoid remains show clear affinities with the Nagri fauna of the Pakistan Siwaliks. Biochronological correlations with the Potwar Plateau based on suoids indicate an age bracket of ~10-9 Ma for the ‘Lower Alternations’ of Haritalyangar, close to the bracket mostly recently proposed on the basis of magnetic polarity stratigraphy.

    Table and Figures | Reference | Related Articles | Metrics | Comments0
    New findings of Xiyuichthys (Xiushuiaspidae, Galeaspida) from the Silurian of Jiangxi Province and Tarim Basin
    SHAN Xian-Ren, LIN Xiang-Hong, ZHANG Yu-Meng, LI Xu-Tong, GAI Zhi-Kun
    Vertebrata Palasiatica    2023, 61 (4): 245-260.   DOI: 10.19615/j.cnki.2096-9899.230904
    Abstract723)   HTML260)    PDF(pc) (15245KB)(521)       Save

    New findings of the early Silurian Xiyuichthys (Xiushuiaspidae, Galeaspida), Xiyuichthys lixiensis sp. nov. and X. zhangi are described from the Qingshui Formation in Jiangxi Province and the Tataertag Formation in Tarim Basin respectively. X. lixiensis sp. nov. is characterized by the partially serrated lateral margin of the headshield and the ornamentation composed of extremely coarse granular tubercles (one tubercle per square millimetre). The complete early Silurian biostratigraphic sequence in northwestern Jiangxi warrants the erection of a standard section for the correlation of Silurian shallow marine red beds in South China and Tarim blocks. Thus, the finding of X. lixiensis from the Qingshui Formation (Silurian Lower Red Beds) in Jiujiang of Jiangxi bears important biostratigraphic significance. It can directly compare to X. zhangi from the Tataertag Formation in Tarim Basin on the specific level, which corroborates the correlations between the Tataertag Formation in Tarim Block and the Silurian Lower Red Beds in South China. Fossil records suggest that Xiushuiaspidae have a relatively broader stratigraphic range, but exhibit distinct composition at different stratigraphic horizons, with Xiyuichthys and Changxingaspis arising in the Silurian Lower Red Beds (Qingshui, Tangchiawu, and Tataertag formations) and Xiushuiaspis occurring in the Silurian Upper Red Beds (Xikeng Formation).

    Table and Figures | Reference | Related Articles | Metrics | Comments0
    First histochemical examination of a Miocene ostrich eggshell with the oldest mineral-bound peptides
    WU Qian, PAN Yan-Hong, LI Zhi-Heng, ZHOU Zhong-He, Alida M. BAILLEUL
    Vertebrata Palasiatica    2024, 62 (2): 120-134.   DOI: 10.19615/j.cnki.2096-9899.240329
    Abstract452)   HTML26)    PDF(pc) (4148KB)(515)       Save

    Because ancient proteins have a higher preservation potential than ancient DNA, proteomic studies can help shed light on the biology of some extinct biological groups that are beyond the reach of the field of ancient DNA. The oldest peptide discovered so far is part of the protein struthiocalcin (SCA-1) involved in eggshell mineralization and found within an ostrich egg from the Late Miocene Linxia Basin of Northwest China. It was originally hypothesized that SCA-1 was evenly distributed within the eggshell and was able to enter the fossil record for so long, because it was bound to calcite crystals. We conducted histological, scanning electron microscopy and Raman spectroscopic analyses on this same fossil egg to test if any protein or organic matter could be observed within specific regions of the eggshell and indeed bound to calcite crystals. Our results show that the eggshell is made entirely of calcite except at the base layer, which is made of mammillary knobs at least partially made of apatite. These knobs were secondarily phosphatized during diagenesis. After decalcification of this material, the fossilized mammillary knobs showed fibrous residues consistent in location and morphology with remnants of original organic material forming a network. This network was similar to the organic matrix observed in an extant ostrich eggshell with this same method. The results here suggest that SCA-1 may have been concentrated at the mammillary knobs, rather than evenly throughout the eggshell. Phosphatization may be another taphonomic process that favors organic preservation in deep-time. The paleoclimate and taphonomic environment of the Linxia Basin may have provided favorable conditions for the molecular preservation of this egg. More in-depth histochemical and mineralogical analyses will certainly increase our understanding of organic and ancient protein preservation in this basin.

    Table and Figures | Reference | Related Articles | Metrics | Comments0
    Taxonomic revision of Sinoeugnathus kueichowensis (Halecomorphi, Holostei) from the Middle Triassic of Guizhou and Yunnan, China
    FENG Dong-Hao, XU Guang-Hui, MA Xin-Ying, REN Yi
    Vertebrata Palasiatica    2023, 61 (3): 161-181.   DOI: 10.19615/j.cnki.2096-9899.230703
    Abstract1737)   HTML506)    PDF(pc) (51651KB)(503)       Save

    The previously alleged ‘eugnathid amiiform’ Sinoeugnathus kueichowensis is a small-sized halecomorph from the Middle Triassic (Ladinian) marine deposits of Guizhou and Yunnan, China. A morphological redescription and taxonomic revision of this taxon are provided based on a detailed examination of the holotype and 15 new specimens. Studies of these specimens revealed some morphological details previously undescribed or misidentified for this taxon, including a hatchet-shaped antorbital, two broad suborbitals, a sensory canal in the maxilla, and three pairs of extrascapulars. For the first time, Sinoeugnathus was incorporated into an analysis of halecomorph phylogeny, and the results recover it as the sister taxon of the Anisian Subortichthys from Luoping, Yunnan, and both are grouped with two Ladinian genera Allolepidotus and Eoeugnathus from the Monte San Giorgio area into a monophyletic group (namely Subortichthyidae fam. nov. herein) at the base of Ionoscopiformes. This taxonomic reassessment of Subortichthys provides new insights into the phylogeny and paleogeographic evolution of Ionoscopiformes.

    Table and Figures | Reference | Supplementary Material | Related Articles | Metrics | Comments0
    A giant bamboo rat from the latest Miocene of Yunnan
    Lawrence J. FLYNN, LI Qiang, Jay KELLEY, Nina G. JABLONSKI, JI Xue-Ping, Denise F. SU, WANG Xiao-Ming
    Vertebrata Palasiatica    2023, 61 (4): 277-283.   DOI: 10.19615/j.cnki.2096-9899.230710
    Abstract723)   HTML30)    PDF(pc) (718KB)(493)       Save

    The Shuitangba subbasin lignite deposits of the Zhaotong Basin in northern Yunnan Province have produced vertebrate fossils of terminal Miocene age. We conducted test wet screening of fossiliferous sediment in 2014 to increase representation of small mammals. This effort produced four teeth of a very large bamboo rat, much larger than the previously known bamboo rat present at Shuitangba, and representing a new species. This new species is characterized by its molars being remarkably larger than those of other known species of Miorhizomys , and being hypsodont with cementum, and less anterorposteriorly compressed. The age of this new species from Shuitangba is in the range of 6.2 to 6.7 Ma. It appears that diverse bamboo rats of the extinct genus Miorhizomys were present in the Late Miocene of Yunnan, somewhat before the 6 Ma appearance of extant Rhizomys to the north in the vicinity of Shanxi Province.

    Table and Figures | Reference | Related Articles | Metrics | Comments0
    The first description of Equidae (Perissodactyla, Mammalia) from Xinyaozi Ravine in Shanxi, North China
    DONG Wei, BAI Wei-Peng, LIU Wen-Hui, ZHANG Li-Min
    Vertebrata Palasiatica    2023, 61 (3): 212-244.   DOI: 10.19615/j.cnki.2096-9899.220926
    Abstract546)   HTML33)    PDF(pc) (14734KB)(445)       Save

    Abundant mammalian fossils were uncovered during the field exploration for Nihewan beds at the beginning of the 1980s along Xinyaozi Ravine at Nangaoya Township of Tianzhen County, Shanxi Province in North China. But most equid material was not yet described except that of Equus stenonis. Six forms of Nihewanian equids were confirmed from the Xinyaozi specimens in the present study, five of which were described for the first time. They include four stenonids such as Equus sanmeniensis, E. teilhardi, E. huanghoensis and E. stenonis, and two hipparionines such as Hipparion (Proboscidipparion) sinense and H. (Plesiohiparrion) shanxiense. The diversification of stenonids in the Early Pleistocene was significant in North China with four taxa in Xinyaozi alone. The persistence of Neogene relics such as hipparionines was still present in the Early Pleistocene with two hipparionine taxa in Xinyaozi. Equus sanmeniensis and H. (Proboscidipparion) sinense were two representative equids not only coexisted in the Early Pleistocene but also widely distributed in China. The diversity of equids also implies the diversified vegetation on which they depended. The hypsodont dentitions and well developed cement, as well as completely molarized premolars of Xinyaozi equids indicate their abrasive diet mostly on monocotyledonous and grassland habitats with considerable scales enough to nourish six taxa of equids.

    Table and Figures | Reference | Related Articles | Metrics | Comments0
    Occurrence of “Hippotherium” in the Old World: a revision of two hipparion species in Eurasia
    SUN Bo-Yang, LIU Yan, WANG Shi-Qi, DENG Tao
    Vertebrata Palasiatica    2025, 63 (1): 57-80.   DOI: 10.19615/j.cnki.2096-9899.241120
    Abstract344)   HTML22)    PDF(pc) (1765KB)(440)       Save

    A controversial taxon, Hipparion plocodus, is reviewed in the present study. Hi. plocodus has been confirmed to be a valid species with definite diagnostic characteristics, represented by cranial specimens from Baode, Shanxi Province. The phylogenetic analysis performed in the present study, with a new matrix, shows that Hi. plocodus forms a monophyletic group with a European species, Hippotherium malpassii. Actually, no close relationship between so-called Hm. malpassii and the genus Hippotherium has been identified, and the record of stratigraphic range of this genus in late stage of Late Miocene is currently absent. Herein previously Hi. plocodus and Hm. malpassii have both attributed into “Hipparion” before the discovery of better material. Evolutionary stages and correlative absolute age showed that these two species should derive independently from some primitive clade. During the late stage of the Late Miocene, the development of the Asian summer monsoon enhanced the humidity of China, with forest and wood habitats expanding considerably under this setting. As the result, one Eurasian closed-habitat lineage thus extended its range into China, which had become very suited for it, give rise to “Hi.plocodus.

    Table and Figures | Reference | Supplementary Material | Related Articles | Metrics | Comments0
    Reappraisal of Bothriolepis sinensis Chi, 1940 from the Tiaomachien Formation, Hunan, China
    LUO Yan-Chao, ZHU Min, LU Li-Wu, PAN Zhao-Hui
    Vertebrata Palasiatica    2023, 61 (4): 261-276.   DOI: 10.19615/j.cnki.2096-9899.230901
    Abstract784)   HTML32)    PDF(pc) (21874KB)(386)       Save

    Bothriolepis sinensis Chi 1940, mainly based on anterior median dorsal plates from the Middle Devonian Tiaomachien Formation of Hunan, is the first Paleozoic vertebrate taxon erected in China. Although additional materials of B. sinensis from the type locality were described by Lu in 1988, its morphology and phylogeny remain poorly understood. In this study, we complemented the morphology of the skull and trunk armor of B. sinensis based on Chi’s specimens housed in the Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, and several previously undescribed specimens in the Geological Museum of China. Bothriolepis sinensis differs from other Bothriolepis in the following combination of characteristics: enlarged supraotic thickening, length/width ratio of head shield 1.4-1.6, broad orbital fenestra (greater than 1/3 of the head shield width), and fan-shaped preorbital recess. The phylogenetic analysis did not place B. askinae in the most basal position of the genus and revealed that B. sinensis and B. kwangtungensis consistently from a monophyletic group characterized by their slender proximal segment of the pectoral fin (length/width ratio greater than 7). A majority of Chinese Bothriolepis species (B. niushoushanensis , B. lochangensis , B. tungseni , B. kwangtungensis and B. sinensis ) were clustered in a clade characterized by the pectoral pit-line on the ventral central plate 1 extending to the ventral central plate 2. The paleogeographic reconstruction using the data from the DeepBone platform showed that Bothriolepis had its oldest occurrences in South China and East Gondwana in Eifelian, dispersed rapidly worldwide, and then diversified across the coasts of the Rheic Ocean.

    Table and Figures | Reference | Supplementary Material | Related Articles | Metrics | Comments0
    First discovery of Neogene proboscidean fossils in southeast China
    LI Chun-Xiao, TANG Jian-Rong, WANG Shi-Qi, WANG Lin-Chang, ZHENG Ying-Kai, DENG Ke, LIN Min, CHEN Run-Sheng, ZHOU Guo-Wu, CHEN Zhong-Yang
    Vertebrata Palasiatica    2025, 63 (1): 43-56.   DOI: 10.19615/j.cnki.2096-9899.241110
    Abstract340)   HTML18)    PDF(pc) (3333KB)(352)       Save

    Stegolophodon is an age-informative genus of mammals that had a widespread distribution during the Neogene. This paper reports the discovery of Stegolophodon fossils from the Middle Miocene lower Fotan Formation at the Zhangpu locality, Fujian Province, China. This discovery represents the first evidence of Neogene proboscidean fossils in southeastern China. The newly found molar materials have low tooth crowns, very straight lophs/lophids, and an indistinct median sulcus. The mesoconelets and posterior cingulum are well-developed, while the second posterior pretrite central conule is significantly reduced. These specimens closely resemble Stegolophodon pseudolatidens in cheek tooth morphology, and can thus be attributed to the same species. This discovery fills a gap in the fossil record of large mammals in this region during the Neogene and provides valuable insights into the evolution of proboscideans and paleoenvironments.

    Table and Figures | Reference | Related Articles | Metrics | Comments0
    An egg clutch of the Stalicoolithidae discovered in Wuning, Jiangxi, China
    ZHOU Ming-Xiao, YAN Yun, QIU Wen-Jiang, FANG Kai-Yong, ZHU Xu-Feng, WANG Qiang, WANG Xiao-Lin
    Vertebrata Palasiatica    2023, 61 (4): 317-325.   DOI: 10.19615/j.cnki.2096-9899.230519
    Abstract551)   HTML16)    PDF(pc) (10584KB)(304)       Save

    Here we describe an incomplete dinosaur clutch with three broken eggs and seven prints discovered in Wuning County, Jiangxi Province, that can be referred to Coralloidoolithus shizuiwanensis based on the following features: the eggs are nearly spheroid and arranged tightly and irregularly in the clutch, the eggshell thickness ranges 2.76-2.97 mm, the horizontal accretion lines are almost evenly distributed throughout the eggshell, and the secondary eggshell units are distributed in the medial and outer zones of the columnar layer. This egg clutch of Coralloidoolithus shizuiwanensis represents the first discovery of dinosaur eggs in Wuning County, and shows the age of the strata containing the dinosaur eggs in this area should be Late Cretaceous.

    Table and Figures | Reference | Related Articles | Metrics | Comments0
    Micromammal fossils from the basal part of the Jiaozigou Formation in Yagou area, Linxia Basin, Gansu Province
    WANG Ban-Yue, QIU Zhan-Xiang
    Vertebrata Palasiatica    2023, 61 (4): 284-316.   DOI: 10.19615/j.cnki.2096-9899.230927
    Abstract407)   HTML17)    PDF(pc) (19072KB)(281)       Save

    Renewed fieldwork in 2003 produced a rich micromammal assemblage from the basal part of the Jiaozigou Formation in the Yagou area of Linxia Basin. 17 genera distributed among 13 families of three orders were recovered. The micromammal fauna is a typical Oligocene assemblage for Central and Eastern Asia. 14 genera (~82% of the fauna) are common in the Oligocene of Asia. Of them four genera and four species of Eucricetodon are restricted to the Oligocene, one genus (Bagacricetodon ) is restricted to Late Oligocene and Glis and Eomyodon made their first appearances in the Late Oligocene. Based on this micromammal composition, the basal part of the Jiaozigou Formation in the Yagou area could be mainly of Late Oligocene in age, which is in accordance with the conclusion based on large mammal fossils. In comparison with the other Late Oligocene micromammal faunas in Central and East Asia, the Yagou Fauna is slightly older than the Ulan III biozone of Nei Mongol and biozone C of Mongolia, because it has two Eocene genera and lacks more advanced genera. This is roughly in accordance with the recent palaeomagnetic interpretation for the Maogou section, where the lower boundary of the Jiaozigou Formation was correlated with Chron C10r (~29 Ma). The presence of large number of xerophilous zapodines, ctenodactylids, cricetids and lagomorphs combined with fossorial Tsaganomys and the lithology of the fossil-bearing deposits, composed of gypsiferous reddish brown mudstone, tend to show a semiarid woodland-shrubland habitat during the Late Oligocene in Yagou area. In Late Oligocene more frequent faunal interchange might have occurred between Asia and Europe (4 genera commonly shared) rather than between Asia and America (only 1 genus shared), partly because of the disappearance of the Turgai Strait.

    Table and Figures | Reference | Related Articles | Metrics | Comments0
    Reinvestigation of Yuanotherium minor and its implications for the cuspal homology and maxillary-palatal evolution of tritylodontids
    LIU Lu, REN Ji-Cheng, MAO Fang-Yuan
    Vertebrata Palasiatica    2025, 63 (2): 81-101.   DOI: 10.19615/j.cnki.2096-9899.250331
    Abstract294)   HTML15)    PDF(pc) (8111KB)(200)       Save

    Several tritylodontid taxa have been reported from the Upper Jurassic of the Wucaiwan area in the Junggar Basin of Xinjiang, northwestern China, including Yuanotherium minor. The original study described the partially preserved postcanine teeth in the middle of the left upper maxilla. After detailed re-examination of the specimen and by CT scanning, 3D reconstruction, and scanning electron microscopy observations, we provided a more detailed description of the osteology, neurosensory, and tooth wear pattern for all the bones preserved in this specimen and clarified some characters. Based on new information about the cusp wear pattern, the chewing movement pattern of the dentition and detailed cusp morphology, we discussed the cuspal homology of upper cheek teeth of tritylodontids and postulate a standardized method for cusp identification. We hypothesize that the unique maxilla characteristics furnish the evidence for transitional stages about the evolution of the upper jaw-palate structure in tritylodontids.

    Table and Figures | Reference | Related Articles | Metrics | Comments0
    The Pleistocene mammalian forest dwellers in monsoon dominated provinces of China as forest dynamics proxies
    BAI Wei-Peng, DONG Wei, ZHANG Li-Min, LIU Wen-Hui
    Vertebrata Palasiatica    2025, 63 (2): 133-158.   DOI: 10.19615/j.cnki.2096-9899.250311
    Abstract158)   HTML21)    PDF(pc) (3485KB)(167)       Save

    Monsoon has an important impact on the development of vegetation that subsequently has significant influence on the evolution of plant consumers. The diversities of forest dwellers or herbivores follow the evolution of the vegetation, and it is therefore possible to take such diversities as forest or vegetation dynamic proxies. The present work selected 36 Pleistocene faunas of large mammals from monsoon-dominated provinces in China as materials and calculated the diversities of forest dwellers and herbivores with different approaches, as well as the consensus gradient coefficients of all the selected faunas in different flora regionalized subkingdoms. The results show that with the evolution and transitions of the East Asian summer and winter monsoon intensities, the forest vitality decreased while steppe vitality increased gradually in a fluctuated way from the Early Pleistocene to the Late Pleistocene, especially in the provinces north of the Qinling-Huaihe Line. The analyses of such diversities of the faunas can help to determine the forest dynamic proxies. Moreover, the correlation of such proxies to loess-paleosol sequences and marine isotope stages can in turn help to improve the accuracy of dating fauna ages and paleoenvironment reconstruction.

    Table and Figures | Reference | Supplementary Material | Related Articles | Metrics | Comments0
    Early Miocene micromammal fossils from Gucheng in Linxia, Gansu, China
    WANG Ban-Yue, QIU Zhu-Ding, LI Lu
    Vertebrata Palasiatica    2025, 63 (2): 102-132.   DOI: 10.19615/j.cnki.2096-9899.250417
    Abstract162)   HTML12)    PDF(pc) (12030KB)(99)       Save

    The micromammal fossils collected from the Shangzhuang Formation of the Linxia Basin, Gansu, are described here. The assemblage consists of 16 species of 13 genera belonging to 7 families, including one new species and one taxon previously unknown from China. Among them 5 genera are Oligocene holdovers and 11 genera/species are known to make their first appearances in Early Miocene, indicating an Early Miocene age for the Gucheng Fauna. The absence of Oligocene survivors such as Tataromys, Yindirtemys, Eucricetodon and Tachyoryctoides, which usually occur in the Xiejian age of Early Miocene, and the presence of newcomers Protalactaga, Megacricetodon and Gobicricetodon, that made their first appearance only in the Shanwangian age of late Early Miocene, suggest that the Gucheng Fauna is of a later age of Early Miocene. The new species, Sinolagomys guchengensis, showing more derived morphology than in S. ulunguensis, seems to support an assessment of the fauna in Shanwangian age. Thus, the Gucheng Fauna may belong to late Early Miocene Shanwangian, partially equivalent to MN 3/4 of the European land mammal zonation. Ecological analysis of the fauna indicates that the palaeoecological condition of the Gucheng area might still be a predominantly arid shrub-steppe in late Early Miocene.

    Table and Figures | Reference | Related Articles | Metrics | Comments0